Thermal model of lava in Mt. Agung during December 2017 episodes derived from Integrated SENTINEL 2A and ASTER remote sensing datasets

dc.contributorHáskóli Íslandsen_US
dc.contributorUniversity of Icelanden_US
dc.contributor.authorAufaristama, Muhammad
dc.contributor.authorHöskuldsson, Ármann
dc.contributor.authorJónsdóttir, Ingibjörg
dc.contributor.authorUlfarsson, Magnus
dc.contributor.authorErlangga, I G D
dc.contributor.authorThordarson, Thorvaldur
dc.contributor.departmentJarðvísindastofnun (HÍ)en_US
dc.contributor.departmentInstitute of Earth Sciences (UI)en_US
dc.contributor.departmentJarðvísindadeild (HÍ)en_US
dc.contributor.departmentFaculty of Earth Sciences (UI)en_US
dc.contributor.departmentRafmagns- og tölvuverkfræðideild (HÍ)en_US
dc.contributor.departmentFaculty of Electrical and Computer Engineering (UI)en_US
dc.contributor.schoolVerkfræði- og náttúruvísindasvið (HÍ)en_US
dc.contributor.schoolSchool of Engineering and Natural Sciences (UI)en_US
dc.date.accessioned2019-09-09T12:53:33Z
dc.date.available2019-09-09T12:53:33Z
dc.date.issued2019-08-14
dc.descriptionPublisher's version (útgefin grein)en_US
dc.description.abstractIn the beginning of December 2017, Mt. Agung eruption powered down to minor ash emissions and on the middle of December, aerial photographs of the crater were taken by Indonesia Centre of Volcanology and Geological Hazard Mitigation (PVMBG) showing a steadily growing lava occupying approximately one third of the crater. 3D digital elevation model (DEM) of crater were created by PVMBG during and before the eruption, corresponded to lava volume around 2 x 10−2 km3 has been filled the crater. Here we present a method for deriving thermal model within the lava during eruption on 8 and 9 December 2017 using observations from multi infrared satellite SENTINEL 2A and Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER). We use Thermal Eruption Index (TEI) based on the Shortwave infrared (SWIR) on SENTINEL 2A and Thermal Infrared (TIR) on ASTER, allowing us to differentiate thermal domain within the lava. This study has successfully produced model of sub-pixel temperature (Th), radiant flux (Φrad) and crust thickness model of lava (Δh). The subpixel temperature and radiant flux during the eruption is in the range 655 to 975 °C and 179 MW respectively. The crust thickness model of the lava in the range of 9 to 14 m and the total volume of lava crust during this period is estimated at 3 x 10−3 km3. The combination of infrared satellite remote sensing data shows a potential for fast and efficient classification of difference thermal domains and derive thermal model of lava.en_US
dc.description.sponsorshipThe first author has been supported by the Indonesia Endowment Fund for Education (LPDP), Institute of Earth Science and Vinir Vatnajökuls during his PhD project.en_US
dc.description.versionPeer Revieweden_US
dc.format.extent012016en_US
dc.identifier.citationAufaristama, M., Hoskuldsson, A., Jonsdottir, I., Ulfarsson, M. O., Erlangga, I. G. D., & Thordarson, T. (2019). Thermal model of lava in Mt. Agung during December 2017 episodes derived from Integrated SENTINEL 2A and ASTER remote sensing datasets. OP Conference Series: Earth and Environmental Science, 311, 012016. doi:10.1088/1755-1315/311/1/012016en_US
dc.identifier.doi10.1088/1755-1315/311/1/012016
dc.identifier.issn1755-1307
dc.identifier.issn1755-1315 (eISSN)
dc.identifier.journalIOP Conference Series: Earth and Environmental Scienceen_US
dc.identifier.urihttps://hdl.handle.net/20.500.11815/1239
dc.language.isoenen_US
dc.publisherIOP Publishingen_US
dc.relation.ispartofseriesIOP Conference Series: Earth and Environmental Science;311
dc.rightsinfo:eu-repo/semantics/openAccessen_US
dc.subjectHraunen_US
dc.subjectHraunrennslien_US
dc.subjectFjarkönnunen_US
dc.titleThermal model of lava in Mt. Agung during December 2017 episodes derived from Integrated SENTINEL 2A and ASTER remote sensing datasetsen_US
dc.typeinfo:eu-repo/semantics/articleen_US
dcterms.licenseContent from this work may be used under the terms of the Creative Commons Attribution 3.0 licence. Any further distribution of this work must maintain attribution to the author(s) and the title of the work, journal citation and DOI.en_US

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